The Student's Elements of GeologyLyell, Charles, Sir
Science
The Student's Elements of Geology
Lyell, Charles, Sir
Geology
Fig. 155: Cinnamomum Rossmässleri.
American Character of the Flora.—If we consider not merely the number
of species but those plants which constitute the mass of the Lower
Miocene vegetation, we find the European part of the fossil flora very
much less prominent than in the Œningen beds, while the foreground is
occupied by American forms, by evergreen oaks, maples, poplars, planes,
Liquidambar, Robinia, Sequoia, Taxodium, and ternate-leaved pines.
There is also a much greater fusion of the characters now belonging to
distinct botanical provinces than in the Upper Miocene flora, and we
shall find this fusion still more strikingly exemplified as we go back
to the antecedent Eocene and Cretaceous periods.
Professor Heer has advocated the doctrine, first advanced by Unger to
explain the large number of American genera in the Miocene flora of
Europe, that the present basin of the Atlantic was occupied by land
over which the Miocene flora could pass freely. But other able
botanists have shown that it is far more probable that the American
plants came from the east and not from the west, and instead of
reaching Europe by the shortest route over an imaginary Atlantis,
migrated in an opposite direction, crossing the whole of Asia.
Arctic Miocene Flora.—But when we indulge in speculations as to the
geographical origin of the Miocene plants of Central Europe, we must
take into account the discoveries recently made of a rich terrestrial
flora having flourished in the Arctic Regions in the Miocene period
from which many species may have migrated from a common centre so as to
reach the present continents of Europe, Asia, and America. Professor
Heer has examined the various collections of fossil plants that have
been obtained in North Greenland (lat. 70°), Iceland, Spitzbergen, and
other parts of the Arctic regions, and has determined that they are of
Miocene age and indicate a temperate climate.[2] Including the
collections recently brought from Greenland by Mr. Whymper, the Arctic
Miocene flora now comprises 194 species, and that of Greenland 137
species, of which 46, or exactly one-third, are identical with plants
found in the Miocene beds of Central Europe. Considerably more than
half the number are trees, which is the more remarkable since, at the
present day, trees do not exist in any part of Greenland even 10
degrees farther south.
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